served from IRI/LDEO Climate Data Library
∫dY ∂T ∫dY [ IGOSS nmc Reyn_SmithOIv2 weekly sst ] : ∂T Sea Surface Temperature data
weekly sst sst sst int_dY partial_T int_dY ∂T Sea Surface Temperature from IGOSS nmc Reyn_SmithOIv2: SST fields updated from version 1 with more COADS data, new sea-ice to SST conversion algorithm, and 1971-2000 climatology.Independent Variables (Grids)
- Time (time)
- grid: /T (julian_day) ordered [ (12-18 Nov 1981) (19-25 Nov 1981) (26 Nov 1981 - 2 Dec 1981) ... (22-28 Jan 2023)] N= 2151 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (1E) to (0) by 1.0 N= 360 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (90S) to (90N) by 1.0 N= 181 pts :grid
Other Info
- CE
- 35
- colorscalename
- sstcolorscale
- CS
- -2
- datatype
- realarraytype
- units
- 3.52566458086469×10-09 degree_Kelvin radian2 north second-1
- colorscale
References
Reynolds_etal2002Last updated: Wed, 22 Mar 2023 18:04:56 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $integral dY$ $partialdiff sub T$ $integral dY$ [ IGOSS nmc Reyn_SmithOIv2 weekly sst ] [ X Y | T] | M | M | M |
|---|
Filters
Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.- Monthly Climatology calculates a monthly climatology by averaging over all years.
- anomalies calculates the difference between the (above) monthly climatology and the original data.
- Integrate along X Y T
- Differentiate along X Y T
- Take differences along X Y T
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units